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Defining an aristotype crystal structure and crystallographic distortions in leucite/pollucite-structured phases with space group \(Ia\overline {3} d\)

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Abstract

A universal aristotype crystal structure for leucite/pollucite-structured phases (A2B2IIIC4IVO12, A2BIIC5IVO12) with space group \(Ia\overline {3} d\) has been determined by a non-linear optimisation of the fractional coordinates. The resultant T-site tetrahedron exhibits close to perfect \(\overline {4} 3m\) point group symmetry (quadratic elongation 1.0000124, tetrahedral angle variance 1.53 × 10−5 degrees2). For any distorted leucite/pollucite crystal structure, an associated aristotype phase can be derived from the optimised fractional coordinates, with the aristotype phase lattice parameter calculated from the volume of the hettotype T-site tetrahedron. Assuming the aristotype T-site tetrahedron to be ideal, the distortion of the hettotype tetrahedron from that of the aristotype is described as the linear sum of the amplitudes of an appropriate set of symmetry-adapted basis-vectors of the effective regular TO4 molecule consistent with the observed point group symmetry within the crystal structure. The methodology is illustrated by reference to the disordered T-site, leucite-structured phase K2MgSi5O12.

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Acknowledgements

KSK is grateful to Prof. J. M. Perez-Mato (University of the Basque Country) for his help and advice in carrying out this work, and to Prof. L. Elcoro (University of the Basque Country) for guidance with the similarity transformation of the E irreducible representation. Prof. A. M. Glazer (University of Oxford), and Prof. S. W. Lovesey (Science and Technology Facilities Council) are thanked for e-mail correspondence. The manuscript has been improved by the comprehensive review by Prof. G. D. Gatta and an anonymous reviewer; Prof. Milan Rieder is thanked for editorial assistance.

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Knight, K.S., Henderson, C.M.B. Defining an aristotype crystal structure and crystallographic distortions in leucite/pollucite-structured phases with space group \(Ia\overline {3} d\). Phys Chem Minerals 46, 595–605 (2019). https://doi.org/10.1007/s00269-019-01025-1

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